Beginning in 1958, the American scientist Charles David Keeling established continuous, high-precision measurements of atmospheric carbon dioxide concentration at the Mauna Loa Observatory in Hawaii, chosen for its high altitude and distance from major local sources of pollution that could distort readings. The resulting record, known as the Keeling Curve, revealed both a small seasonal oscillation driven by the growth and die-back of Northern Hemisphere vegetation and a steady year-on-year rise in carbon dioxide concentration, providing the first unambiguous, continuously measured evidence that atmospheric carbon dioxide was increasing as a result of human activity. The measurements have continued essentially unbroken since 1958 and remain the longest direct record of atmospheric carbon dioxide, foundational to the modern scientific understanding of human-driven climate change.
Facts
MethodContinuous measurement with an infrared spectrophotometer (nondispersive infrared sensor) 1 Key FindingShowed the first significant evidence of rapidly increasing carbon dioxide levels in the atmosphere 1 LocationMauna Loa Observatory, Hawaii 1 Sources
1. Keeling Curve (Wikipedia)
Lead section, sentence 1 (year clause)
from 1958 to the present day
Lead section, sentence 1 (location clause)
Mauna Loa Observatory on the island of Hawaii
Lead section, sentence 3
showed the first significant evidence of rapidly increasing carbon dioxide (CO2) levels in the atmosphere
Mauna Loa measurements section
infrared spectrophotometer, now known as a nondispersive infrared sensor
In Group: Weather and Climate Experiments, Lead
is a graph of the annual variation and overall accumulation of carbon dioxide in the Earth's atmosphere based on continuous measurements taken at the Mauna Loa Observatory on
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